Crustal structure across the post-spreading magmatic ridge of the East Sub-basin in the South China Sea: Tectonic significance
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文摘

The 2D velocity structure corresponds to oceanic crust affected by post-spreading magmatism.

The low velocity body might correspond to extrusive rocks intercalated with sedimentary layers.

The Jixiang seamount maybe formed by the buoyancy-driven upwelling mechanism.

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